Quantum States of Neutrons in the Gravitational Field
Claude Krantz
January 2006
i
Quantum States of Neutrons in the Gravitational Field: We present an ex- periment performed between February and April 2005 at the Institut Laue Langevin (ILL) in Grenoble, France. Using neutron detectors of very high spatial resolu- tion, we measured the height distribution of ultracold neutrons bouncing above a reflecting glass surface under the effect of gravity. Within the framework of quan- tum mechanics this distribution is equivalent to the absolute square of the neutron’s wavefunction in position space.
In a detailed theoretical analysis, we show that the measurement is in good agreement with the quantum mechanical expectation for a bound state in the Earth’s gravitational potential. We further demonstrate that the results can neither be explained within the framework of a classical calculation nor under the assumption that gravitational effects can be neglected. Thus we conclude that the measurement manifests strong evidence for quantisation of motion in the gravitational field as is expected from quantum mechanics and as has already been observed in another type of measurement using the same experimental setup.
Finally, we study the possibilities of using the mentioned position resolving mea- surement in order to derive upper limits for additional, short-ranged forces that would cause deviations from Newtonian gravity at lenght scales below one millime- ter.
Quantenzust¨andevon Neutronen im Gravitationsfeld Es wird ein Experi- ment vorgestellt, das von Februar bis April 2005 am Institut Laue Langevin (ILL) in Grenoble, Frankreich, durchgef¨uhrtwurde. Dabei wurde mit Hilfe von Neutro- nendetektoren mit sehr hoher Ortsaufl¨osungdie H¨ohenverteilung ultrakalter Neu- tronen gemessen, die unter dem Einfluss der Schwerkraft ¨uber einer reflektierenden Glasoberfl¨ache h¨upfen. In der Quantenmechanik entspricht diese H¨ohenverteilung dem Betragsquadrat der Ortswellenfunktion eines Neutrons.
Eine genaue Analyse der Messdaten ergibt, dass sich diese in guter Uberein-¨ stimmung mit der quantenmechanischen Erwartung f¨ureinen gravitativ gebunde- nen Zustand befinden. Es wird gezeigt, dass die Messergebnisse weder rein klassisch, noch unter Vernachl¨assigungdes Schwerepotentials beschreiben werden k¨onnen.Aus dieser Tatsache wird geschlossen, dass das Experiment starke Hinweise auf eine Quantisierung der Bewegung im Gravitationsfeld liefert, wie sie von der Quanten- mechanik vorhergesagt wird und in systematisch anderen Messungen mit dem selben experimentellen Aufbau bereits nachgewiesen wurde.
Schließlich wird untersucht, inwiefern aus besagten ortsaufl¨osendenMessungen Obergrenzen f¨urzus¨atzliche, kurzreichweitige Kr¨afteabgeleitet werden k¨onnen.Sol- che Kr¨aftew¨urden– bei Abst¨andenunterhalb eines Millimeters – Abweichungen vom Newton’schen Gravitationsgesetz bewirken. ii Contents
Introduction 1
1 Ultracold Neutrons and Gravity 3
1.1 The Neutron ...... 3
1.1.1 Fundamental Interactions ...... 3
1.1.2 Ultracold Neutron Production ...... 5
1.1.3 Interaction of Ultracold Neutrons with Surfaces ...... 8
1.2 Gravity and Quantum Mechanics ...... 10
1.2.1 The Schr¨odingerEquation ...... 10
1.2.2 Airy Functions ...... 11
1.2.3 The WKB Approximation ...... 13
1.2.4 Remarks ...... 14
2 The Experiment 17
2.1 Overview of the Installation ...... 17
2.2 The Waveguide ...... 19
2.3 Integral Flux Measurements ...... 22
2.4 Position Sensitive Measurements ...... 23
2.4.1 The CR39 Nuclear Track Detector ...... 24
iii iv CONTENTS
2.4.2 The Measurements ...... 26
2.4.3 The Data Extraction Process ...... 26
2.4.4 Data Corrections ...... 29
3 Quantum Mechanical Analysis 33
3.1 Observables of the Measurement ...... 33
3.1.1 Quantum Mechanical Position Measurement ...... 34
3.1.2 Time Dependence ...... 35
3.2 The Quantum Mechanical Waveguide ...... 38
3.2.1 Eigenstates ...... 38
3.2.2 Transitions within the Waveguide ...... 43
3.2.3 The Scatterer ...... 45
3.3 A First Attempt to Fit the Experimental Data ...... 47
3.3.1 The Fit Function ...... 48
3.3.2 Fit Results ...... 49
3.3.3 Groundstate Suppression Theories ...... 51
3.4 The Starting Population ...... 52
3.4.1 Transition into the Waveguide ...... 52
3.4.2 The Collimating System ...... 55
3.4.3 The Energy Spectrum ...... 58
3.4.4 Starting Populations ...... 59
3.5 Fit to the Experimental Data ...... 60
3.5.1 The 50-µm Measurement (Detector 7) ...... 61
3.5.2 The 25-µm Measurement (Detector 6) ...... 63 CONTENTS v
4 Alternative Interpretations 65
4.1 Classical View of the Experiment ...... 65
4.1.1 Classical Simulation of the Waveguide ...... 66
4.1.2 Classical Fit to the 50-µm Measurement ...... 69
4.2 The Gravityless View ...... 73
4.2.1 The Waveguide without Gravity ...... 73
4.2.2 Gravityless Fit to the 50-µm Measurement ...... 77
5 Gravity at Small Length Scales 83
5.1 Deviations from Newtonian Gravity ...... 83
5.2 A Model of the Experiment including Fifth Forces ...... 86
5.2.1 Fitting the Experimental Data ...... 87
5.2.2 Discussion of the Fit Results ...... 89
Summary 93
Bibliography 95 vi CONTENTS Introduction
What is gravity? In many respects this may be one of the most important questions ever asked. Answers to it have always been milestones on the way from ancient natural philosophy to modern science. Every physicist knows the legendary free fall experiments of Galileo Galilei at the dawn of empiricism, forshadowing Newton’s later formalism of the attraction of masses, itself the very starting point of modern physics and science as a whole.
Since then, our comprehension of nature has changed. And paradoxally, the ques- tion that triggered it all is still one of the most obscure. The Standard Models of Cosmology and Particle Physics describe our world up to its largest and down to its smallest scales. Doubtlessly, both of these theories deserve being considered among the grandest cultural achievements in the history of mankind. Yet, they stand sepa- rate. The presently adopted view of gravity is provided by Einstein’s General Theory of Relativity and has been unchallenged for almost a century. During this time, par- ticle physics has firmly established that the three non-gravitational interactions are governed by the principles of quantum physics, which are inherently incompatible to the classical field concept of General Relativity. The latter is therefore expected to, sooner or later, have to be replaced by a quantised theory of gravity.
Since 1999, an experiment at the Institut Laue Langevin in France is redoing Galilei’s free fall experiments using as probe mass an elementary particle: the neu- tron. Although earlier attempts using atoms have been undertaken, this experiment is the first to have detected quantum states in the gravitational field by observing, at very high spatial resolutions, the motion of ultracold neutrons under the effect of gravity [Nesv02]. Its results may be considered as a first timid step on the way to bridge the gap separating gravitation and quantum physics.
This diploma thesis presents a further measurement performed in 2005 using the mentioned experiment. By means of position resolving detectors, we directly imaged the height distribution of neutrons bouncing, under the effect of gravity, a few tens of micrometers above a reflecting surface. Within the framework of quantum mechanics, this distribution is equivalent to the absolute square of the neutron’s wavefunction in position space.
1 2 INTRODUCTION
In a first chapter of this text, we develop the basic concepts of quantised motion of an elementary particle in the field of gravity as they can be derived from quantum mechanics. Additionally, we provide the fundamentals of neutron physics as far as they are relevant to our experiment. Special attention is payed to the unique properties of ultracold neutrons, without which the mentioned measurement would be impossible to realise. The latter is throughoutly described in chapter 2, where we give an overview of the experimental techniques put into operation and discuss the data taking processes.
The main focus of this thesis lies on chapter 3, where we further develop the re- sults from the first chapter into a detailed theoretical description of the experiment and the measurement process. Within the framework of quantum mechanics, this yields a prediction of the density distribution of low-energetic neutrons bouncing under the effect of gravity. In order to rule out possible misinterpretations of the data, we subsequently oppose this quantum mechanical expectation to two alterna- tive ones described in chapter 4: The first neglects the effects of quantum mechanics, the second those of gravity. All three models are compared to the neutron height distributions that have actually been measured.
Over the last years, a number of theories have arisen which, in an effort to derive a quantum description of gravity, predict deviations from the Newtonian gravitational potential at length scales below one millimeter [Ark98] [Ark99]. Thus, in a last chapter, we study possible upper limits on such deviations that could be obtained from the type of measurement we have performed. Chapter 1
Ultracold Neutrons and Gravity
1.1 The Neutron
Over the last decades the neutron has has become a tool of ever increasing impor- tance to both the fields of fundamental and applied physics.
With a rest mass m = 939.485(51) MeV/c2, the neutron is the second-lightest member of the baryon octet. As such, it can in principle be used to probe all four of the fundamental interactions. While this is not astonishing in itself, there are a few notable properties that do make the neutron special among all baryons: It is electrically neutral, easy enough to produce and sufficiently long-lived to be a very practical probe particle.
Additionnally, neutrons may be cooled down to kinetic energies of less than 1 meV, which are then of the same order of magnitude than the potentials of their fundamental interactions. At the latter we will have a closer look in the following subsection.
1.1.1 Fundamental Interactions
Neutrons are electrically neutral. In the valence quark model, the neutron consists of one up and two down quarks and therefore carries an electric charge equal to 0. The most precise measurement of the neutron charge was performed by G¨ahler et al. by observing the deviation of a neutron beam in an electrostatic field [G¨ahl89]. The experiment yields −21 qn = (−0.4 ± 1.1) · 10 e
3 4 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY with e being the electron charge magnitude. It’s neutrality renders the neutron immune to otherwise all-overwhelming electromagnetic forces and ensures the possi- bility to probe other, weaker interactions on low energy scales. It makes the neutron the particle of choice for low-energy physics [Abe02], in contrast to its charged coun- terpart the proton, typically used in high-energy experiments which overcome the dominion of electromagnetism at the expense of enormous energy densities.
This having been said, the neutron does take part in electromagnetic interac- tions through its magnetic moment ~µn. It’s interaction potential with an external magnetic field B~ reads Vmag = −~µn · B.~
The neutron magnetic moment is proportional to the nuclear magneton ~µN:
~µn = −1.9130427(4) ~µN itself linked to the proton mass mp
e¯h −8 µN = |~µN| = ≈ 3.152 · 10 eV/T . 2mp
Thus a neutron inside an exterior magnetic field has got a potential energy of
Vmag ≈ 60 neV/T.
Weak interaction manifests itself most notably through the fact that the free neutron is unstable. It decays spontaneously into a proton, an electron and an anti-electron-neutrino:
− n −→ p + e +ν ¯e (+782 keV) . (1.1)
Since the proton is the only baryon with lower rest mass than the neutron and since the energy release is to low to produce heavy leptons, there are no other decay channels. The decay being governed by weak interaction, the mean lifetime of a neutron is still quite long. The world average value as of 2004 is [Pdg04]
τn = (885.7 ± 0.8) s
This time is long enough to provide the opportunity to use neutrons in low-energy storage experiments.
Being, alongside with the proton, the constituent of atomic nuclei, the neutron obviously also takes part in strong interactions. A free neutron may be scattered at or absorbed into the strong potential of a nucleus. Neutrons coupling only very weakly to electromagnetic fields, strong scattering is the standard way of manipulating them. With the help of suitably crafted strong potentials, neutrons may be reflected 1.1. THE NEUTRON 5 at surfaces, guided along tubes, cooled or heated into predefined kinetic energy spectra.
Strong interaction is also the key to neutron detection: Particle detectors are typically sensitive to ionising particles only. The neutron being electrically neutral, it usually needs to be converted, i.e. absorbed into a nucleus which in turn reacts by either emission of γ-rays or charged particles. These can then be detected through their electromagnetic interaction with surrounding matter.
Within the framework of this text, we are mainly interested in gravitational interaction of neutrons with the Earth. Given its mass m = 1.67495 · 10−27 kg [Pdg04], a neutron’s potential energy as a function of altitude z evaluates to
neV V (z) = mgz ≈ 100 · z[m] m
For a neutron, a kinetic energy of 100 neV corresponds to a velocity v ≈ 2.2 m/s. This means that slow neutrons may be significantly accelerated or decelerated by falling or raising in the Earth’s gravitational field. It is noteworthy that gravity can easily be the strongest long-ranged interaction affecting the neutron. The strong in- teraction being short-ranged and Vmag being weak and easily controlled by magnetic shielding, low energetic neutrons are prime candidates for the observation of gravi- tational effects in systems formed by elementary particles. The quantum mechanics arising from this will be discussed in quite extensive a manner in section 1.2.
1.1.2 Ultracold Neutron Production
As indicated above, free neutrons have a lifetime of approximately a quarter of an hour. There is therefore little hope of finding them in large quantities in nature as is true for protons and electrons which are readily available in the form of hydrogen. Neutrons naturally only occur tightly packed in degenerate, strongly-interacting Fermi gases. In such systems it is possible that the β-decay (1.1) would be net endothermic and therefore cannot take place. Nature manifests two realisations of this situation: In atomic nuclei both neutrons and protons form degenerate Fermi gases bound in their common strong potential well. For stable (i.e. non-β-active) nuclei the energy amount required in order to add a proton to the system is greater than the 782 keV released by the reaction (1.1), as a result, the decay is thermo- dynamically prohibited. At sufficiently high matter densities, the strong binding potential may be replaced by a gravitational one. Inside neutron stars, remnants of red supergiants, neutrons are subject to gravity fields so intense that the increase in volume of the system related to neutron decay would require a rise in gravitational potential energy of more than 782 keV. With diameters of order ten kilometres, such stars therefore almost exclusively consist of neutrons with no possibility to decay. 6 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY
For obvious reasons neutron stars could never be very practical devices for labo- ratory use. The spectrum of possible neutron sources for experimental ends therefore reduces to atomic nuclei. There are a number of isotopes (e.g. 252Cf) that produce free neutrons through spontaneous fission reactions. Such sources are small and easy to maintain but of low intensity. In order to get high neutron fluxes, one has to turn towards sources involving induced nuclear reactions. Among these there are two main types: Spallation sources consist of a particle accelerator ‘firing’ onto a target made of heavy nuclei. Given a suitable choice of isotopes, the incident particle is absorbed into the target nucleus which reacts to this excitation by evaporation of neutrons. Although several spallation sources worldwide are expected to come into operation in the near future, any powerful neutron sources available today provide stimulated neutron emission through the use of nuclear fission reactors.
The neutron source of the Institut Laue-Langevin (ILL) located in Grenoble (France), at which the experiment described hereafter was performed, is of this latter type. We shall therefore explain the production of neutrons on the basis of this particular setup depicted in figure 1.1. Independently of the reaction being spontaneous or induced, neutrons emerging from a nuclear fission process will always carry high kinetic energies of order 1 MeV. The core of the reactor at the ILL consists of a highly-enriched uranium fuel element immersed into a heavy water tank. Each fission reaction produces an average number of 2.4 neutrons. Close to the core the neutron flux density is of the order of 1015 cm−2s−1. By strong scattering at the deuterons contained in the heavy water (D2O), these high energetic neutrons are thermalised, i.e. the temperature of the neutron gas adapts itself to that of the D2O- moderator which is kept at a constant value of 300 K by heat-exchange with a light water reservoir.
One part of these thermal neutrons is used up in the production of further fission reactions in the fuel material, the other part is piped through neutron guides towards the instrumentation halls surrounding the reactor building. Having energies around 25 meV, corresponding to wavelengths of approximately 2 A,˚ these neutrons are mainly used in scattering experiments of solid state physics.
For some types of experiments slower neutrons are needed. In a “cold source”, another, smaller moderator tank filled with liquid deuterium (D2) cooled down to 25 K, the neutrons are further decelerated to have energies of approximately 2 meV and are then called cold neutrons.
Experiments like the one to be described in this text rely on neutrons of even much lower energy: Very cold neutrons (VCN, few µeV) and ultracold neutrons (UCN, below 0.3 µeV). These cannot be obtained through thermalisation but have to be selected from the lowest energetic tail of the cold Maxwellian spectrum. This is done by vertically extracting the neutrons using a curved guide (see figure 1.1). The curvature ensures that incident angles of neutrons onto the guide’s walls are 1.1. THE NEUTRON 7
Figure 1.1: The UCN source at the ILL: The illustration shows the fuel element (1), the D2O-moderator tank (2) itself immersed into the light water tank (3), the cold source (4) from which cold neu- trons are vertically extracted and piped through the curved VCN guide (5) and the turbine (6) feeding UCN experiments. (picture taken from www.ill.fr)
large. Neutrons with velocities above a threshold vmax are unable to follow the guide as they will penetrate the wall material rather than be reflected at its surface. At the exit of the curved guide, located 13 m above the cold source, only very cold and ultracold neutrons are present.
The particle density in the UCN part of the spectrum is then enhanced by means of the so-called UCN turbine. The turbine consists of 690 nickel coated blades revolving inside a vacuum chamber connected to the curved guide in such a way that they recede from the VCN beam at half the speed of the arriving neutrons. Upon collision with the blades VCN therefore loose longitudinal momentum in the laboratory frame and are slowed down into the UCN regime. It should be emphasised that the turbine cannot enhance the phase space density in the UCN energy interval 8 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY above its value inside the cold source. This is in agreement with Liouville’s theorem: In a thermodynamically closed system, the phase space density is constant for all times. The turbine is therefore designed to only repopulate the phase space volume of UCN that have been lost on their way from the cold source.
1.1.3 Interaction of Ultracold Neutrons with Surfaces
Ultracold neutrons have the faculty of being totally reflected at a wide range of material surfaces under any incident angle. As this unique feature is of crucial importance to the experiment discussed hereafter, we want to gain some insight into the underlying principles. As indicated above, the dominating effect in the interaction of neutrons with matter is strong scattering between neutrons and atomic nuclei.
Let us sketch very briefly the mechanism of scattering at a nucleus, a detailed calculation can be found e.g. in [Gol91]: An ultracold neutron with kinetic energy E ≤ 100 neV is characterised by a de Broglie wavelength of h λ = √ ≥ 90 nm . (1.2) 2mE The strong potential of a nucleus can be approximated by a spherical square well potential: ½ −V : r ≤ R V (r) = 0 (1.3) nuc 0 : r > R The strong interaction being very short ranged, R is about equal to the radius of the nucleus of order 1 fm and the depth of the well V0 is approximately 40 MeV. If we represent the incident neutron by a plane wave, the overall wave function in free space has got the form ikr ~ e ψ = eik·~r + f(θ) (1.4) r as derived in any standard text on quantum mechanics [Schwa98]. We call θ the scattering angle and f(θ) the scattering amplitude which contains the matrix ele- ment of the interaction and thereby depends on the shape of the potential Vnuc(r). However, because of λ À R, we expect the reflected wave to be of spherical shape (s-wave scattering), which means that f(θ) will not contain any angular dependence:
f(θ) = −a . (1.5)
We call a the scattering length of the nucleus. It is obvious that a has to have the dimension of a length as from scattering theory one derives that |f|2 is the differential cross-section of the process: dσ = |f(θ)|2 dΩ 1.1. THE NEUTRON 9
In our case f is independent of the solid angle and the total scattering cross-section reads 2 σtot = 4πa .
The question arises how to link the measurable quantity a to the scattering potential Vnuc(r). It is in principle not possible to use perturbation theory to describe the scattering process, as the perturbation V0 is much larger than the neutron energy E. However, the range of the potential Vnuc(r) is limited to R and we are only interested in the shape of the wave function at r À R, i.e. well outside the range of interaction, where the wave function can be assumed to be only lightly disturbed. In 1936 Fermi found that under these circumstances Vnuc(r) may be replaced by an effective, delta-shaped potential [Gol91]
2π¯h2a U (r) = δ(3)(~r) , (1.6) F m where m is the mass of the scattered neutron and a the scattering length. Named Fermi Potential after it’s creator, UF permits to compute the scattering matrix elements in the Born approximation.
A slow neutron impinging onto condensed matter will now feel the superposition of the nuclei’s individual Fermi potentials:
2π¯h2 X U(~r) = a δ(3)(~r − ~r ) . (1.7) m i i i
At each ~ri scattering produces a spherical reflected wave. For ultracold neutrons, the wavelength λ 3 orders of magnitude larger than the distances separating the nuclei. Interaction will therefore take place through a large number of simultaneous scattering processes and equation (1.7) can be approximated by a homogeneous Fermi potential 2π¯h2 U(~r) ≈ U = · a¯ · n , m where the sum over the δ-distributions has been replaced by the particle density n of the material anda ¯ is the averaged scattering length of the nuclei. U may be regarded as a macroscopic property of the material. In the last step we have thereby reduced our complicated scattering problem to a very simple and yet quite correct mathematical description. The normal motion component of a neutron hitting a smooth material surface can now be described as one dimensional scattering of a free particle state at a step potential. For a large variety of materials, |U| is larger than the typical energy of an ultracold neutron (≤ 100 neV). Their surfaces then correspond to potential barriers impenetrable to the particles.
In the experiment discussed hereafter, neutrons bounce above glass surfaces. Optical glass essentially consists of silicon dioxide which is characterised by a Fermi 10 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY potential of
Uglass ≈ 100 neV. Thus ultracold neutrons can safely be assumed to be totally reflected at its surface.
In fact, UCN may even be defined as being those neutrons which are totally reflected from the inner walls of neutron guides at all angles of incidence.
1.2 Gravity and Quantum Mechanics
The experiment discussed hereafter measures the gravitational free fall of neutrons over very small length scales. The dynamics of low-energetic elementary particles being naturally governed by non-relativistic quantum mechanics, we are therefore facing the problem of solving the Schr¨odingerequation in the case of a gravitational potential.
Although we shall later have to refine and generalise the results obtained from the following treatment and although the problem of a linear potential is throughoutly discussed in many standard texts on quantum mechanics [Fl¨u99],it is useful to address it at this early stage as it allows us to develop most of the concepts needed in the later chapters of this text.
1.2.1 The Schr¨odingerEquation
Consider a system formed by the Earth and a particle gravitationally bound to it. Let ME and m be the masses of Earth and particle respectively. According to Newton’s Law, the potential energy of such a system is
M m V˜ (r) = −G E , (1.8) r where r denotes the distance separating the two centres of mass and G the gravi- tational constant. We are interested in the case where the particle is located at a height z above the surface of the Earth which is very small compared to the planet’s radius RE: r = RE + z with z ¿ RE Equation (1.8) can then be expanded up to the first order in z:
M m M V˜ (z) ≈ −G E + G E mz (1.9) R R2 | {z E } | {zE} =V˜ (RE ) =:g 1.2. GRAVITY AND QUANTUM MECHANICS 11
Dropping the additive constant to the left, we finally write V (z) = mgz , where g is the Earth’s gravitational acceleration at sea level as defined in equation (1.9). The Hamiltonian of the above system therefore writes p2 H = + mgz . 2m It may be worth pointing out that in the last step we have identified inertial and gravitational mass, i.e. we assume that the Weak Equivalence Principle holds for our system.
This leads to the following time-independent Schr¨odingerequation for the par- ticle’s probability amplitude in position space ψ(z): µ ¶ ¯h2 ∂2 − + mgz ψ(z) = E ψ(z) (1.10) 2m ∂z2 In order to simplify mathematical expressions, it is useful and quite common to introduce a scaling factor R given by
µ ¶1/3 ¯h2 R := (1.11) 2m2g and to define the dimensionless quantities z E ζ := ; ² := . (1.12) R mgR Substituting z → ζ and E → ² in equation (1.10) yields µ ¶ ¯h2 1 ∂2 − + mgRζ ψ(ζ) = mgR² ψ(ζ) , 2m R2 ∂ζ2 and according to the definition (1.11) of R this leads to the following dimensionless eigenvalue equation: µ ¶ ∂2 − + (ζ − ²) ψ(ζ) = 0 (1.13) ∂ζ2
1.2.2 Airy Functions
The differential equation (1.13) is well known in mathematics. Its eigenfunctions are linear combinations of the Airy Functions Ai and Bi. The Airy Functions are transcendental mathematical objects which can be expressed in terms of Bessel Func- tions. For our purposes, we may safely regard them as ‘normal’ real-valued functions with the two notable properties depicted in figure 1.2: 12 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY
1 Ai(ζ−ε) Bi(ζ−ε) 0.8
0.6
0.4
0.2
0
-0.2
-0.4
-12 -10 -8 -6 -4 -2 0 2 ζ−ε
Figure 1.2: The Airy Functions Ai and Bi
1. For ζ → −∞ both Ai and Bi manifest a sin(ζ)-like oscillating behaviour. 2. For ζ → +∞ their behaviours are radically different: Ai converges exponen- tially fast towards 0 while Bi diverges at the same pace.
Armed with this knowledge, we can return to our Schr¨odingerequation. The most general solution ψ(ζ) of (1.13) has the form:
ψ(ζ) = cA Ai(ζ − ²) + cB Bi(ζ − ²) (1.14)
As usual in quantum mechanics, the possible values for the coefficients cA and cB are determined by the boundary conditions of the system at hand. We shall have to return to this point at a later stage but, for now, let us consider the case of the particle falling freely above a reflecting floor placed at z = 0. In addition, the wave function must be normalisable in order to be a Hilbert-vector. Thus we request ψ(ζ) = 0 (ζ ≤ 0) (1.15) ψ(ζ) → 0 (ζ → +∞) (1.16) This system is often referred to as the ‘quantum bouncer’. Because of lim Bi(ζ − ²) = +∞ ζ→+∞ the latter condition can only be fulfilled by setting
cB = 0 . 1.2. GRAVITY AND QUANTUM MECHANICS 13
Together with the boundary at z = 0, this means that eigenstates of our system have got the form ½ N −1Ai(ζ − ²): ζ > 0 ψ(ζ) = 0 : ζ ≤ 0 where N −1 is a factor ensuring the normalisation of the functions. Derivability of the solution at ζ = 0 requires Ai(−²) = 0 . (1.17)
Because of the oscillatory nature of Ai, this means that only particular ² ∈ {²n} are allowed. Recalling that E = mgR², we see from equation (1.17) that our system is characterised by a discrete energy spectrum as expected for any quantum mechanical bound state.
1.2.3 The WKB Approximation
Ai being a transcendental function, solutions to equation (1.17) can be found by numerical computation alone. However a very good approximation for the ²n can be given using the Wentzel-Kramers-Brillouin (WKB) method. A detailed description of the procedure can be found e.g. in [Rueß00]. It yields · µ ¶¸ 3π 1 2/3 ²WKB = n − ; n ∈ N∗ (1.18) n 2 4 The relations (1.12) can be used to express the energy spectrum in physical units
WKB WKB En = mgR²n =: mgzn , (1.19) WKB where the entity zn = ²n R corresponds to the classical jump height of a pointlike particle with energy En. The final result for the solutions of the Schr¨odingerequation (1.10) with the boundary conditions given by (1.15) and (1.16) reads ½ ¡ ¢ N −1Ai z − ²WKB : z ≥ 0 ψWKB(z) = R n . (1.20) n 0 : z < 0
Since the WKB method is a semi-classical approximation, one could expect it to be valid only in the limit of very high quantum numbers n. However the energies obtained from (1.18) turn out to deviate from the true eigenvalues by no more than one percent even for the lowest states. In table (1.1) the WKB eigenvalues of the first eigenstates as given by (1.18) are compared to those obtained from a numerical solution of equation (1.17).
Both eigenstates and eigenvalues to the Schr¨odingerequation (1.10) having been found, the ‘quantum bouncer’ is now solved. Adopting the values
m = 1.67495 · 10−27 kg and g = 9.80665 m/s2 14 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY
true WKB true n En [peV] En [peV] ∆E/En [%] 1 1.4067 1.3960 0.76 2 2.4595 2.4558 0.15 3 3.3215 3.3194 0.06 4 4.0832 4.0819 0.03 5 4.7796 4.7786 0.02
Table 1.1: True eigenvalues compared to their WKB approxima- tions for the neutron mass and the gravitational acceleration, equation (1.20) gives the probability amplitude in position space for the free-falling particle for a given quan- tum number n. Figure 1.3 depicts the shapes of the wavefunctions for the first three quantum states.
1.2.4 Remarks
On the Scaling Factor R: In the case of a free falling neutron as described above, the scaling factor R, defined by equation (1.11), evaluates to
R ≈ 5.87 µm .
It is the characteristic length scale of the system and closely related to the Heisenberg Uncertainty Principle, as can be seen as follows [Abe05]: The uncertainty relation for position and momentum reads ¯h ∆z∆p ≥ . (1.21) 2 If we identify the uncertainty of the momentum p with its maximum value and the uncertainty of the position with the classical jump height of the particle, we can write √ p 2 ∆p = pmax = 2mE = 2m g∆z Inserting this into (1.21) leads to
p ¯h ∆z3/2 2m2g ≥ 2 or µ ¶1/3 ¯h2 ∆z ≥ = 4−1/3 R. 8m2g Hence, up to a numerical factor of magnitude O(1), R is equal to the position uncertainty of the bound particle. 1.2. GRAVITY AND QUANTUM MECHANICS 15
400 ψ (z) ψ1 2(z) ψ (z) 300 3
200
100
0
-100
-200
-300 -10 0 10 20 30 40 50 60 z [µm]
Figure 1.3: The probability amplitudes in position space for the WKB first three eigenstates ψn of the ‘quantum bouncer’
On Gravitationally Bound States: In connection with the ‘quantum bouncer’ it is often stated that quantisation of energies arises because the particle is confined inside a cavity formed by the gravitational potential and the potential barrier of the reflecting floor which we have taken to be infinitely high. This potential well is depicted in figure 1.4.
In the above treatment, quantisation indeed arose due to the introduction of the boundary condition (1.15). However this does not mean that the absence of a reflecting floor would result in a continuous energy spectrum. The mathematical need for a confining potential barrier actually arises from the Taylor expansion (1.9) of the potential V˜ (r) which is valid for small absolute values of z only:
˜ ME m ME m V (z) ≈ −G + G 2 z . RE RE It is perfectly possible to solve the Schr¨odingerequation without this limitation, by directly plugging V˜ (r) from equation (1.8) into it. We would then get the standard 1/r central potential problem well-known from the quantum mechanics of the hy- drogen atom. With r being the distance separating the centre of the Earth and the free falling neutron, the particle’s probability amplitude would then be of the form [Schwa98] l+1 −κr 2l+1 un,l(r) ∼ r e Ln+1 (2κr) , where n and l are the principal and angular momentum quantum numbers and L 16 CHAPTER 1. ULTRACOLD NEUTRONS AND GRAVITY
4
3
2 [peV]
1
0
V(z) 0 10 20 30 40 z [µm]
Figure 1.4: The potential well confining the particle and the first three eigenstates
denotes the Associated Laguerre Polynomials. The case of a particle located close to RE would then just correspond to a very high value of n. It can be shown that for large values of n and r, un,l(r) is well approximated by the Airy function Ai we have found under the assumption of a perfectly linear potential.
In classical mechanics one derives parabolic trajectories for free-falling pointlike masses. In fact these are correct only in the case of not-too-high falling altitudes, the general solutions of the problem being Kepler ellipses. In the very same way one might state that the solutions (1.20) are approximations of bound central potential states valid in the homogenous field limit (1.9). Chapter 2
The Experiment
In the preceding chapter we have discussed the behaviour of an elementary particle subject to a linear gravitational potential as it is expected from quantum mechan- ics. Since 1999 our experiment at the Institut Laue Langevin (ILL) analyses this phenomenon empirically by observing the motion of ultracold neutrons falling onto totally reflecting glass mirrors at very high spatial resolutions of the order of 1 µm. The following chapter will describe this setup, will provide an overview of the ex- perimental techniques involved and explain the measurement performed within the framework of this diploma thesis in 2005.
2.1 Overview of the Installation
The experimental setup is mounted on the UCN instrumentation platform PF2 of the ILL, located directly above the reactor core as has been described in section 1.1 (see figure 1.1). In an experiment seeking to observe such faint an effect as quantisation in gravitationally bound neutron states, some care obviously needs to be taken in order to protect the setup against mechanical and electromagnetic perturbations omnipresent inside a research reactor.
As shown in figure 2.1 the setup consists of a vacuum chamber build on top of a massive granitic stone table. Accurately polished and plane to very high standards, this stone supports all the critical components of the setup. The system contains two high precision digital inclinometers normally used in geophysics and rests upon three piezo elements. The inclinometers provide information about the setup’s current inclination with respect to the horizon. This data is fed into a computer which in turn controls the voltage applied to the piezo elements. Working as a closed loop, this inclination control system can actively correct the pitch of the stone table and
17 18 CHAPTER 2. THE EXPERIMENT
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